<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>0124-2253</journal-id>
<journal-title><![CDATA[Revista científica]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. Cient.]]></abbrev-journal-title>
<issn>0124-2253</issn>
<publisher>
<publisher-name><![CDATA[Universidad Distrital Francisco José de Caldas]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0124-22532023000300067</article-id>
<article-id pub-id-type="doi">10.14483/23448350.20963</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Modelado de la sismicidad colombiana como una red compleja espacio-secuencial]]></article-title>
<article-title xml:lang="en"><![CDATA[Modeling Colombian Seismicity as a Complex Spatial-Sequential Network]]></article-title>
<article-title xml:lang="pt"><![CDATA[Modelagem da sismicidade colombiana como uma complexa rede espaço-sequencial]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[León-Vargas]]></surname>
<given-names><![CDATA[Daniel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Bucheli-Guerrero]]></surname>
<given-names><![CDATA[Víctor-Andrés]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ordoñez-Erazo]]></surname>
<given-names><![CDATA[Hugo-Armando]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad del Valle  ]]></institution>
<addr-line><![CDATA[Cali Valle del Cauca]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad del Valle  ]]></institution>
<addr-line><![CDATA[Cali Valle del Cauca]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad del Cauca  ]]></institution>
<addr-line><![CDATA[Popayán Cauca]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2023</year>
</pub-date>
<numero>48</numero>
<fpage>67</fpage>
<lpage>81</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0124-22532023000300067&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0124-22532023000300067&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0124-22532023000300067&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Este artículo busca describir la sismicidad de Colombia utilizando redes complejas, en las cuales los nodos representan redes cúbicas (con latitud, longitud y profundidad) donde ocurren los eventos sísmicos y los enlaces siguen la secuencia temporal de estos eventos. Si bien se han reportado trabajos similares en la literatura, este trabajo incorpora la profundidad para una mejor comprensión de este fenómeno. Esta investigación considera 5797 eventos del catálogo de terremotos del Servicio Geológico de los Estados Unidos (USGS) correspondientes a Colombia y con una magnitud superior a un determinado umbral, los cuales ocurrieron entre enero 1 de 1975 y enero 18 de 2021. Se describe la estructura de la red mediante una comparación entre redes aleatorias y de pequeño mundo. Así, esta estructura brinda información sobre los mecanismos de liberación de energía y las fuentes que recurrentemente producen eventos sísmicos en Colombia. Los resultados muestran que estas redes presentan características de pequeño mundo, independientemente del tamaño de celda o la granularidad utilizados para construirlas. Este hallazgo es consistente con los resultados reportados para la misma región en redes espaciotemporales bidimensionales. Como una red de pequeño mundo, el esfuerzo y la energía de la región se liberan de acuerdo con una estructura caracterizada por la presencia de hubs y sus relaciones dentro de la red en general. Mediante el aprovechamiento de la información obtenida en este estudio, se pueden entrenar modelos de aprendizaje automático que superen los modelos actuales de base para el pronóstico.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract This article seeks to describe the seismicity of Colombia using complex networks, in which the nodes represent cubic cells (with latitude, longitude, and depth) where seismic events occur, and the links follow the temporal sequence of these events. While similar works have been reported in the literature, this study incorporates depth to gain a more detailed understanding of this phenomenon. This research considers 5797 events from the earthquake catalog of the United States Geological Survey (USGS), corresponding to Colombia and with a magnitude greater than a certain threshold, which occurred between January 1, 1975, and January 18, 2021. The network structure is described by comparing random and small-world networks. Thus, said structure provides information about the energy release mechanisms and the sources that recurrently produce seismic events in Colombia. The results show that these networks exhibit small-world properties, regardless of the cell size or granularity used to construct them. This finding is consistent with the results reported for the same region in two-dimensional spatiotemporal networks. As a small-world network, the effort and energy in the region are released according to a structure represented by the presence of hubs and their relationships within the overall network. By leveraging the information obtained in this study, it is possible to train machine learning models that outperform the current baseline forecasting models.]]></p></abstract>
<abstract abstract-type="short" xml:lang="pt"><p><![CDATA[Resumo Este artigo procura descrever a sismicidade da Colômbia usando redes complexas, nas quais os nós representam redes cúbicas (com latitude, longitude e profundidade) onde ocorrem eventos sísmicos e os links seguem a sequência temporal desses eventos. Embora trabalhos semelhantes tenham sido relatados na literatura, este trabalho incorpora profundidade para uma melhor compreensão desse fenômeno. Esta pesquisa considera 5.797 eventos do catálogo de terremotos do Serviço Geológico dos Estados Unidos (USGS) correspondentes à Colômbia e com magnitude superior a um determinado limite, ocorridos entre 1º de janeiro de 1975 e 18 de janeiro de 2021. A estrutura é descrita. por meio de uma comparação entre redes random e small world. Assim, esta estrutura fornece informações sobre os mecanismos de liberação de energia e as fontes que produzem eventos sísmicos recorrentemente na Colômbia. Os resultados mostram que essas redes apresentam características de mundo pequeno, independentemente do tamanho da célula ou da granularidade utilizada para construí-las. Esse achado é consistente com os resultados relatados para a mesma região em redes espaço-temporais bidimensionais. Como uma pequena rede mundial, o esforço e a energia da região são liberados de acordo com uma estrutura caracterizada pela presença de hubs e suas relações dentro da rede global. Aproveitando as informações obtidas neste estudo, os modelos de aprendizado de máquina podem ser treinados para superar os modelos de linha de base atuais para previsão.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[modelado de la sismicidad]]></kwd>
<kwd lng="es"><![CDATA[profundidad de los eventos sísmicos]]></kwd>
<kwd lng="es"><![CDATA[redes complejas]]></kwd>
<kwd lng="es"><![CDATA[redes de sismicidad]]></kwd>
<kwd lng="en"><![CDATA[depth of seismic events]]></kwd>
<kwd lng="en"><![CDATA[complex networks]]></kwd>
<kwd lng="en"><![CDATA[seismicity modeling]]></kwd>
<kwd lng="en"><![CDATA[seismicity networks]]></kwd>
<kwd lng="pt"><![CDATA[modelagem da sismicidade]]></kwd>
<kwd lng="pt"><![CDATA[profundidade dos eventos sísmicos]]></kwd>
<kwd lng="pt"><![CDATA[redes complexas]]></kwd>
<kwd lng="pt"><![CDATA[redes de sismicidade]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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